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Understanding Map Projections

Understanding Map Projections

Understanding Map Projections

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GEOGRAPHIC COORDINATE SYSTEM<br />

Geographic coordinates displayed as if the longitude–latitude<br />

values are linear units. An equivalent projection is<br />

Equirectangular with the standard parallel set to the equator.<br />

DESCRIPTION<br />

The geographic coordinate system is not a map<br />

projection. The earth is modeled as a sphere or<br />

spheroid. The sphere is divided into equal parts<br />

usually called degrees; some countries use grads. A<br />

circle is 360 degrees or 400 grads. Each degree is<br />

subdivided into 60 minutes, with each minute<br />

composed of 60 seconds.<br />

The geographic coordinate system consists of<br />

latitude and longitude lines. Each line of longitude<br />

runs north–south and measures the number of<br />

degrees east or west of the prime meridian. Values<br />

range from -180 to +180 degrees. Lines of latitude<br />

run east–west and measure the number of degrees<br />

north or south of the equator. Values range from +90<br />

degrees at the North Pole to -90 degrees at the South<br />

Pole.<br />

The standard origin is where the Greenwich prime<br />

meridian meets the equator. All points north of the<br />

equator or east of the prime meridian are positive.<br />

USES AND APPLICATIONS<br />

<strong>Map</strong> projections use latitude and longitude values to<br />

reference parameters such as the central meridian,<br />

the standard parallels, and the latitude of origin.<br />

Supported map projections• 59

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